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ÉCOLE POLYTECHNIQUEFÉDÉRALE DE LAUSANNE
L M RLCPC / 9 février 2005
LABORATOIRE DEMÉCANIQUE DES ROCHES
Laboratory tests in rock mechanics
J.-F. Mathier
avril 2000 2
EPFL - LMR
LMR Equipments
g Laboratoryn 500 and 2000 kN Presses n triax cells Hoek, Legep, GDSn Direct shear tests
g 2 test hallsn TRIROC Press 3500 kNn Physical modelling
4 tunnel excavation, face stability4 rockfall4 Impact of falling blocs
avril 2000 3
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500 kN and 2000 kN Presses
avril 2000 4
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Standard tests
g Standard testsn Triaxn Unconfined compression, tractionn Modul E, Poisson coefficient n Indirect shear testn Swellingn Creep
g Database
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0
20
40
60
80
100
0 5 10 15 20
σ 1
σ3
[MPa
]
[MPa]
σ1= σ
3+( σ
3+ ) m* s* a
a = 0.61m* = 91.17s*= 8.66R = 0.99
0
20
40
60
80
100
0 5 10 15 20
σ 1
σ3
[MPa
]
[MPa]
σ1= σ
3+( σ
3+ ) m* s* a
a = 0.50m* = 441.70s*= 216.69R = 0.98
3. Strong tectonised
0
20
40
60
80
100
0 5 10 15 20
σ 1
σ3
[MPa
]
[MPa]
σ1= σ
3+( σ
3+ ) m* s* a
a = 0.70m* = 11.79s*= 1.32R = 0.99
0
20
40
60
80
100
0 5 10 15 20
σ 1
σ3
[MPa
]
[MPa]
σ1= σ
3+( σ
3+ ) m* s* a
a = 0.75m* = 6.14s*= 0.31R = 0.98
1. Poorly tectonised 2. Tectonised
4. Very strong tectonised
Triaxial tests : Behaviour of cataclastic rocks
3Several degrees of tectonisation
3Ex: Quartzitic sandstones
numerous tests
good correlation
Thesis Jean Habimana
avril 2000 6
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Direct shear tests on discontinuities
avril 2000 7
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Swelling
g 3 types of testingg Free swell, swell pressure, Huder-Ambergg Procedure AFNORg Interpretationg Mineralogyg Correlations ?
avril 2000 8
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Creep : experimental device
3 triaxial cells for creep tests
Pressure controls
avril 2000 9
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Geotechnical Database
g Data storagen EXCEL versionn Filemaker searchn ACCESS version in progress
g 6000 samplesn 4000 unconfined compressionn 3400 modul En 2200 brasilian testsn 900 triax
g Types of rocksn 10% igneous rocksn 65% sedimentary rocksn 25% metamorphic rocks
g Geographical distribution
avril 2000 10
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Geotechnical Database
French Switzerland
Structures
• highways
• tunnels
• dams
avril 2000 11
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Special tests
g Special testsn Permeabilityn Acoustic emissionn Fracture toughnessn Abrasivity
avril 2000 12
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Permeability
g Ex: SELFRAC Projectg div. and conv. Permeabilty
in hollow cylinderg Boom clay
n K = 10-12 m/sg Opalinus clay
n K = 10-13 m/s
LVDT
Strain gages
Inner drain
outer drain
jacket
Load cell
Pressure sensor
valve
inner pressure
controller
cell pressure
controller
Outer pressure
controller
personal computer pressures control
volumes and pressures acquisition
Personal computer additional
data acquisition
LVDT
Strain gages
Inner drain
outer drain
jacket
Load cell
Pressure sensor
valve
inner pressure
controller
cell pressure
controller
Outer pressure
controller
personal computer pressures control
volumes and pressures acquisition
Personal computer additional
data acquisition
LVDT
Strain gages
Inner drain
outer drain
jacket
Load cell
Pressure sensor
valve
inner pressure
controller
inner pressure
controller
cell pressure
controller
cell pressure
controller
Outer pressure
controller
Outer pressure
controller
personal computer pressures control
volumes and pressures acquisition
personal computer pressures control
volumes and pressures acquisition
Personal computer additional
data acquisition
avril 2000 13
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Acoustic emission –Kaiser effect
3Crack growth Li 1996
8 cm
16 cm
Preloading
Loading andAE measurement
avril 2000 14
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Fracture toughness
0.0
0.5
1.0
1.5
2.0
2.5
3.0
0 0.02 0.04 0.06 0.08 0.1 0.12 0.14
déplacement vertical [mm]
forc
e [k
N]
5.1maxmin / DFAKCB =
[ ] DSDaDaA oo /)/(85.9/15.784.1 2min ++=1.012.020.026632080
1.09.015.020024060
1.08.313.818322055
taohSLD
a0
h
KCB = 1.02
avril 2000 15
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CERCHAR abrasivity test
70 N
1 cm2
1
21
avril 2000 16
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LCPC Abrasivity test (NF P 94-430-2)
0
0
GPPABR −
=
avril 2000 17
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Abrasivity scales
quartzitevery abrasive20004 - 6
graniteabrasive15002 - 4
gneissmedium abrasive10001 - 2
sandstonepoor abrasive5001
limestone, slatevery poor abrasive00 - 1
Example of rockEvaluationABRICA
avril 2000 18
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Comparison between ICA-ABR
0
300
600
900
1200
1500
1800
0 1 2 3 4 5 6
ICA
LC
PC [g
/ton]
Granodiorit Biotit-Serizit Gneis Granitigneous rocks metamorphic rocks sandstoneOlivine basalt Porphyritic basalt Tholeitic basalt
Ratio ABR / ICA ~ 300
Rocks from Switzerland + Island
avril 2000 19
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Accreditation
g LMS+LMRg ISO 17005g Type Cg Renewed till 2009g Normalisationg Cross tests
avril 2000 20
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Cross tests
g 8 laboratoriesg 4 types of rocks
n Carrare marblen Molassic sandstonen Anhydrit from Bexn Limestone from Sixt (France)
g 4 different tests n Densityn Unconfined compression strengthn Modul En Brasilian test
avril 2000 21
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Unconfined compression
189.9204.3198.3200.9184.8186.4165.7193.1188.5Limestone
104.3101.5105.8104.6100.7107.5106.7103.4104.7Carrare marble
158.1144.0153.0167.5162.9158.8163.2158.6154.8Anhydrit
10.38.912.211.59.19.98.59.812.1Molassicsandstone
MeanL1- L9
L9L8bL8aL7L5L3L2L1
avril 2000 22
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TRIROC Press Thesis F. Pellet
avril 2000 23
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Behaviour of bolted rock mass – F. Pellet
Joint oriented to 45 et 60°
1 à 5 joints
2 types of material(plaster and limestone)
Bolts ø 3mm
avril 2000 24
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Base friction apparatus
avril 2000 25
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Base friction apparatus: example of application
g Excavation of shallow tunnel (Thesis M. Karaca 1991)
avril 2000 26
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Base friction apparatus: example of application
g qualitative simulation of toppling
avril 2000 27
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Shallow tunnel modelling (scale 1:20)